The moon As seen through a telescope. General features The Moon (and other bodies) were originally thought to have an atmosphere And living beings (selenites.

Slides:



Advertisements
Similar presentations
The Sun – Earth - Moon System WELL, MOSTLY THE MOON.
Advertisements

Crater Impact craters are the remains of collisions between an asteroid, comet, or meteorite and the Moon. These objects hit the Moon at a range of speeds,
25.1 ORIGIN AND PROPERTIES OF THE MOON
The Moon Satellite – Any body orbiting a central mass No Atmosphere No temperature regulation Daytime temperature = 400 K (266 F) Nighttime temperature.
Earth-Moon System Section 25.2.
The Moon Astronomy 311 Professor Lee Carkner Lecture 13.
The Moon Astronomy 311 Professor Lee Carkner Lecture 13.
April 4, 2006Astronomy Chapter 8 Cratered Worlds: The Moon and Mercury The Moon is an object of lore and superstition. The Moon is our nearest neighbor,
8 February 2005AST 2010: Chapter 8 1 The Moon & Mercury.
25.1 ORIGIN AND PROPERTIES OF THE MOON DAHS MR. SWEET
EARTH’S MOON Section 3 Prentice Hall Earth Science.
The Moon. MOON FACTS Natural satellite of earth Gravity 1/6 of earth - WHY? No atmosphere - WHY? Temp. difference: 134 C to -170 C -WHY?
The Moon. Theories on moon’s creation The Fission Theory: – Part of earth – Thrown out due to extreme rotation – Basin in Pacific Ocean – Earth’s gravity.
The Moon. What is the Moon? A natural satellite One of more than 96 moons in our Solar System The only moon of the planet Earth.
Section 1: Earth’s Moon Preview Key Ideas Exploring the Moon
Moon, Moon Phases & Eclipses. The Moon Calendar The current standard calendar is solar calendar (Gregorian calendar) – counting days The moon phases.
What We Learned this Quarter. What is the Moon? A natural satellite One of more than 96 moons in our Solar System The only moon of the planet Earth.
Formation of the Moon What properties were known about the moon prior to Apollo? Orbital Period Mass and Size and therefore Density Gravity was 1/6 as.
A look at our nearest neighbor in Space! The Moon.
Formation Maria vs. Highlands Maria is Latin for “seas”. These areas appear dark and have smooth relatively crater free surfaces. They represent the.
Internal Heating: Planets and Moons July 21, 2005 Presented to teachers in TRUST by Denton S. Ebel Assistant Curator, Meteorites Department of Earth and.
I. The Highlands  Surface feature that is light in color, high in elevation (mountainous), and heavily cratered.
A look at our nearest neighbor in Space! The Moon Free powerpoints at
8 TH GRADE SCIENCE THE MOON. HOW WAS THE MOON FORMED? It is about 4.6 billions years old. (Same age as Earth) Scientists have measured the age of the.
Photo taken near the landing site of Apollo 17. Crescent Moon.
Chapter 22 Section 3 Earth’s Moon. Earth vs. Moon 3,475 km 12,756 km Earth has 1 natural satellite  the Moon No specific name other than Moon Unusual.
What is the moon like?. The mood is dry and airless and has an irregular surface. Compared to Earth, the moon is small and has large variations in surface.
The Earth-Moon System The Earth’s Atmosphere
Friday October 1, 2010 (Earth’s Moon and Lunar History)
A look at our nearest neighbor in Space! The Moon Free powerpoints at
The Moon and Mercury: Airless Worlds Please take your assigned transmitter And swipe your student ID for attendance tracking.
Sponge – What is a synchronous orbit?. Surface Features - Maria - oceans or seas. (Galileo thought they were oceans when he saw them through his.
Planetary image interpretation and mapping Phil Stooke USGS map I-515.
The Moon.
22.3 Earth Science : Earth’s Moon
1/14/ The Moon - Facts Size km across - 1/4 the size of Earth (like a tennis ball compared to a basketball) Average Distance from Earth.
Earth’s Moon - Luna. Lunar surface features There are 5 basic surface features.
The Moon Origins And Features. Lunar Formation Models The moon is a sister world that formed in orbit around Earth as the Earth formed. The moon formed.
American Unmanned Mission: Surveyor ( )
CHAPTER 1.4 – EARTH’S MOON. IMPORTANT FACTS The first person to truly see the surface of the Moon was Galileo in Galileo used a compound telescope.
What can you see on the Moon with Eyes, Binoculars, Telescopes CYA 30 th January 2016 By Daniel Coe
The Moon. Moon: Basic Facts Diameter: 3500 km (2100 miles) Average Distance: 380,000 km (240,000 miles) Distance range: 360,000 – 400,000 km Orbital eccentricity:.05.
The Surface of the Moon. Surface Surface: The top or outside of something.
Exploring NASA’s Moon Rocks, Lunar Soil Samples & Meteorite Disks!!
Earth’s Moon Ch. 1, Sec. 4. Galileo Italian scientist Viewed the moon through a telescope – Made by putting two lenses in a wooden tube First to view.
Unit 4: The Moon Mr. Ross Brown Brooklyn School for Law and Technology.
The Moon The Earth's moon is not the largest satellite in the solar system. However, it is closer in size to its planet than any other satellite (with.
22 Chapter 22 Starter 1.How long does it take the moon to cycle through its 8 phases? 2.Describe a solar eclipse. 3.Describe a lunar eclipse. 4.______________.
Homework 1. Is there a good scientific question? 2. Is there a good explanation for why the topic/question is worthy of research? 3. Is there a good hypothesis.
The Moon. Formation Hypotheses Co-Accretion – Earth and Moon formed near each other at same time. Fission – Rapidly rotating Proto-Earth released material.
A look at our nearest neighbor The Moon. What is the Moon? A natural satellite One of more than 96 moons in our Solar System The only moon of the planet.
A look at our nearest neighbor in Space! The Moon.
Earth’s Moon. Moon Facts The moon is about 230,000 miles from the Earth Its diameter is 2360 miles which makes it the fifth largest moon in the solar.
Moon Notes Chapter 2 Section 2.
The Moon “Jupiter! I did a song! You ain’t got one!” "Camembert?"
The Moon.
The Moon’s Features.
THE MOON.
Moon Info Created by a real “bum”.
What landforms here on Earth do you think we see on the Moon too?
Moon & Moon Phases.
22.3 – Earth’s Moon.
Section 4 – pg 488 Earth’s Moon
Notes The Moon.
The Moon Astronomy 311 Professor Lee Carkner Lecture 13.
Description of… The Moon.
Sponge – What is a synchronous orbit?
Section 1: Earth’s Moon.
DAVID SHAMAHS & MICHEAL BAKER
Chapter 25 – The Moon Section 25.1
Presentation transcript:

The moon As seen through a telescope

General features The Moon (and other bodies) were originally thought to have an atmosphere And living beings (selenites on the Moon) Therefore, it was assumed that water and land existed Easy to see on the Moon Names of features go back to 17 th C

Lunar oceans Mare (singular), maria (plural) –Dark –Smooth –Low –Often circular –Often large (Imbrium ~1100 km) –Therefore, they had to be water

Highlands Lighter in color (reflectivity/albedo) Rough High (as much as 25,000 ft) Irregular in shape Thought to be the continental areas

Minor features Craters –Microscopic to few hundreds of km –Many clearly visible by naked eye –Seen by Galileo –Named after scientists, philosophers of antiquity (and others) Valleys –In the highlands –Not common

Minor features Rilles –Sinuous Like empty river beds –Straight Long linear valleys Rays –Bright streaks radial to craters –Small to large

Minor features Regolith –Lunar soil –Gravelly –Difficult to see real bed rock

Gross features – EarthMoon –Density –Gravity 11/6 –Escape V –(Km/sec)

First (Serious) Study of Moon 1962 Shoemaker and Hackmann Shoemaker – geologist Hackmann – geographer Assumption –Maria formed by enormous impacts –Law of superposition holds for the Moon –Mare material is basalt lava

Law of superposition Simple case – sedimentary rocks

Application to impact

S and H chose Mare Imbrium –Northeast part of the near side –Large circular mare –Surrounded by mountains

Maria on the near-side of the Moon

Immediate vicinity of Mare Imbrium

Procedure Isolate the area including M Imbrium And the surrounding region –Specifically –Copernicus –Eratosthenes Determine the sequence of events

Time Absolute –Specify the age in time units –Example: the Onondaga limestone was formed 380 million years ago Relative –Specify the age in non-time units –Example: the Edwardian age in England –The Elizabethan age

Argument M. Imbrium was formed by impact Created ejecta blanket If Copernicus was older, it would have been buried But Copernicus is visible Therefore, Copernicus is younger than the impact that formed M. Imbrium

Further, M. Imbrium is filled with lava Therefore, the lava came after the impact that formed M. Imbrium Copernicus is situated on some of the mare material Therefore, Copernicus is younger that the lava

Chronology of the Moon Sequence of events The time units are named (relative time) Names are taken from the feature in question Thus, the crater Copernicus was created in Copernican time (note the different spelling)